A novel explainable deep learning framework for reconstructing South Asian palaeomonsoons

IF 3.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Kieran M. R. Hunt, Sandy P. Harrison
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引用次数: 0

Abstract

Abstract. We present novel explainable deep learning techniques for reconstructing South Asian palaeomonsoon rainfall over the last 500 years, leveraging long instrumental precipitation records and palaeoenvironmental datasets from South and East Asia to build two types of model: dense neural networks ('timeline models') and convolutional neural networks (CNNs). The timeline models are trained individually on seven regional rainfall datasets and while they capture decadal-scale variability and significant droughts, they underestimate interannual variability. The CNNs, designed to account for spatial relationships in both predictor and target, demonstrate higher skill in reconstructing rainfall patterns and produce robust spatiotemporal reconstructions. The 19th and 20th centuries were characterised by marked inter-annual variability in the monsoon, but earlier periods were characterised by more decadal- to centennial-scale oscillations. Multidecadal droughts occurred in the mid-seventeenth and nineteenth centuries, while much of the eighteenth century (particularly the early part of the century) was characterised by above-average monsoon precipitation. Extreme droughts tend to be concentrated in south and west India and often coincide with recorded famines. By applying explainability techniques, we show that the models make use of both local hydroclimate and synoptic-scale dynamical relationships. Our findings offer insights into the historical variability of the Indian summer monsoon and highlight the potential of deep learning techniques in palaeoclimate reconstruction.
用于重建南亚古单峰的新型可解释深度学习框架
摘要我们利用来自南亚和东亚的长期仪器降水记录和古环境数据集,构建了两种类型的模型:密集神经网络("时间线模型")和卷积神经网络(CNN),提出了重建过去 500 年南亚古季风降雨量的新型可解释深度学习技术。时间轴模型是在七个地区降雨量数据集上单独训练的,虽然它们能捕捉到十年尺度的变化和重大干旱,但却低估了年际变化。旨在考虑预测因子和目标的空间关系的 CNN 在重建降雨模式方面表现出更高的技能,并产生了稳健的时空重建。19 世纪和 20 世纪的季风具有明显的年际变异性,但更早时期的季风则更多地表现为十年至百年尺度的振荡。17 世纪中叶和 19 世纪出现了十年一遇的干旱,而 18 世纪的大部分时间(尤其是本世纪初)季风降水量高于平均水平。极端干旱往往集中在印度南部和西部,而且往往与有记录的饥荒同时发生。通过应用可解释性技术,我们发现模型既利用了当地的水文气候,也利用了同步尺度的动力学关系。我们的研究结果有助于深入了解印度夏季季风的历史变异性,并凸显了深度学习技术在古气候重建中的潜力。
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来源期刊
Climate of The Past
Climate of The Past 地学-气象与大气科学
CiteScore
7.40
自引率
14.00%
发文量
120
审稿时长
4-8 weeks
期刊介绍: Climate of the Past (CP) is a not-for-profit international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on the climate history of the Earth. CP covers all temporal scales of climate change and variability, from geological time through to multidecadal studies of the last century. Studies focusing mainly on present and future climate are not within scope. The main subject areas are the following: reconstructions of past climate based on instrumental and historical data as well as proxy data from marine and terrestrial (including ice) archives; development and validation of new proxies, improvements of the precision and accuracy of proxy data; theoretical and empirical studies of processes in and feedback mechanisms between all climate system components in relation to past climate change on all space scales and timescales; simulation of past climate and model-based interpretation of palaeoclimate data for a better understanding of present and future climate variability and climate change.
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